Touching the Detachment (Ockov Fault, Barrandian, Czech Republic)

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Authors	ČERNÝ Jan MELICHAR Rostislav KNÍŽEK Martin JANEČKA Jiří
Year of publication	2008
Type	Conference abstract
MU Faculty or unit	Faculty of Science
Citation
Description	The Prague Synform (Ordovician to Devonian) was folded and thrusted during the Variscan orogeny. The paper is focused on one of the thrusts - the Ockov Fault. The creation of a stratigraphic separation diagram and detailed study of new tunnel exposures has brought about the recognition of the eastern prolongation of the fault, as well as its flat-ramp-flat geometry and thrusting nature.
Related projects:	Interactions among the chemicals, environment and biological systems and their consequences on the global, regional and local scales (INCHEMBIOL) Strukturně geologický a paleotektonický vývoj pražské pánve Barrandienu